Listed in: Geology, as GEOL-321
Formerly listed as: GEOL-32
The majority of Earth’s volume is composed of igneous and metamorphic rocks, which originate through processes that operate deep beneath earth’s surface, driven by the movement of tectonic plates. Igneous and metamorphic rocks preserve an interpretable record of the creation and modification of continents, mountain building, earthquakes, and volcanic eruptions. The formation and existence of these rocks, in turn, modulate global volatile cycles, and the evolution of life-forms on earth. In this course, you will explore the processes and environments involved in the genesis of igneous and metamorphic rocks by integrating field and petrographic observations with quantitative applications of experimental data and chemical principles (thermodynamics, major and trace element geochemistry). Two all-day field trips in the Appalachian Mountains – a formerly active convergent plate margin -- will investigate the construction of volcanic arcs and continental crust, as well as how heat and mass are transferred in earth’s lithosphere during mountain building events. Through field and laboratory investigations, students will learn how to read the archive of earth processes as preserved in igneous and metamorphic rocks and make inferences about the implications of their formation for the evolution of the Earth system. Three hours of class and three hours of laboratory per week.
Requisite: GEOL 271. Spring semester. Professors Guevara and Cheney.